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DOI | 10.1016/j.palaeo.2020.109639 |
Macaronichnus and contourite depositional settings: Bottom currents and nutrients as coupling factors | |
Miguez-Salas O.; Rodríguez-Tovar F.J.; De Weger W. | |
发表日期 | 2020 |
ISSN | 0031-0182 |
卷号 | 545 |
英文摘要 | The trace fossil Macaronichnus segregatis degiberti (7–15 mm in diameter) is recorded for the first time in deep-marine contourites which were deposited in a Late Miocene outer-shelf to upper slope of the Rifian Corridor (Morocco). Macaronichnus is typical of shallow-marine, mainly foreshore environments. It is produced by deposit feeding opheliid polychaetes in high to intermediate latitudes. This record supports the significance of bottom current processes on environmental conditions as a major limiting factor affecting the macrobenthic trace maker community. Mediterranean overflow water during the Late Miocene enabled a high nutrient supply to the seafloor, favouring colonization by Macaronichnus producers. Thus, M. s. degiberti should be used as an indicator for nutrient availability instead of mainly a palaeodepth indicator. This finding provides significant information for oceanographic and environmental reconstructions related to contouritic processes, as well as to contourite characterization. © 2020 Elsevier B.V. |
英文关键词 | Contourites; Deep-sea; Food supply; Morocco; Trace fossils |
语种 | 英语 |
scopus关键词 | bottom current; contourite; deep-sea organism; deposit feeding; depositional sequence; environmental conditions; factor analysis; food supply; marine environment; Miocene; nutrient dynamics; trace fossil; Morocco; Opheliidae; Polychaeta |
来源期刊 | Palaeogeography, Palaeoclimatology, Palaeoecology
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文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/150569 |
作者单位 | Departamento de Estratigrafía y Paleontología, Universidad de Granada, Avd. Fuentenueva s/n, Granada, 18002, Spain; Department of Earth Sciences, Royal Holloway University of London, Egham, TW20 0EX, United Kingdom |
推荐引用方式 GB/T 7714 | Miguez-Salas O.,Rodríguez-Tovar F.J.,De Weger W.. Macaronichnus and contourite depositional settings: Bottom currents and nutrients as coupling factors[J],2020,545. |
APA | Miguez-Salas O.,Rodríguez-Tovar F.J.,&De Weger W..(2020).Macaronichnus and contourite depositional settings: Bottom currents and nutrients as coupling factors.Palaeogeography, Palaeoclimatology, Palaeoecology,545. |
MLA | Miguez-Salas O.,et al."Macaronichnus and contourite depositional settings: Bottom currents and nutrients as coupling factors".Palaeogeography, Palaeoclimatology, Palaeoecology 545(2020). |
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